3.2. Thermal Behaviour
Figure 3 shows the thermal curves obtained from the differential thermal analysis, and
Table 2 gives a summary of T
g, T
c,on, T
liq, and K
H values of the samples. The three formulas containing microelements had higher glass transition, crystallization, and liquidus temperatures than F
0. Glass F
3 had higher values of T
g and T
liq. For the two glasses F
1 and F
2, it can be seen that they had close values of T
g, which is due to the Ionic Field Strength (IFS) of Fe and Mn (IFS = z/r
2, where r is the ionic radius, and z is the valence cation), being IFS equal to 0.16 and 0.15 for Fe and Mn, respectively, according to Dietzel [
34]. The increase in the glass transition temperature, which depends on the number and strength of the cross-links between oxygen atoms and the cation, and the density of covalent cross-linking, plays an important role in understanding the physical properties of glasses. This increase in Tg reflects a strengthening of the structure and increased network stability [
35].
The DTA curves show multiple or broad crystallization and melting peaks. There is some evidence for the presence of multiple phases inside the glass matrix, or the network is constituted from different phosphate species [
36]. The introduction of microelements in the phosphate glass matrix increased K
H from 0.1395 for F
0 to 0.4391, 0.4839, and 0.5279 for F
1, F
2, and F
3 glasses, respectively, which reveals that the thermal stability of these glasses is greater than that of microelements-free glass samples, because the addition of these oxides creates cross-links between phosphate chains which reinforces the network [
35].
3.3. Glass Density
Table 3 summarizes the measured densities of the studied glasses. The densities changed from 3.341 for F
0 to 3.426 for F
3, whereas the molar volumes varied from 33.18 to 32.66 cm
3 mol
−1. Density is sensitive to spatial arrangement and the nature of atoms [
36,
37]. Variations in glass density could illustrate the degree of structural compactness of the glass network. However, in this work, these changes were small and not likely to be significant because most of the microelements incorporated are glass modifiers (expect B
2O
3), principally placed in the holes in the vitreous network [
38].
The calculated molar volumes are shown in
Figure 4. Molar volume, which compares volumes occupied by one mole of glass, is more sensitive to glass structure changes than density as it normalizes for atomic masses of glass components [
27].
The decrease in molar volume by incorporating microelements reflects that the glass structure becomes more compact [
35]. Furthermore, the increase in glass transition temperature (T
g) accompanied by a decrease in the molar volume may reflect an overall increase in the glass network cross-linking [
39].
3.4. Glass Structure
The Raman spectra of the four phosphate glasses, in the range between 200 and 1400 cm
−1, are presented in
Figure 5. It is common knowledge that the phosphate network is built around PO
4 tetrahedral units, which are classified depending on the number of bridging oxygens, using the Q
n designation, where “n” signifies the number of bridging oxygen atoms per tetrahedral unit (n = 0, 1, 2, 3) [
40]. All Raman spectra are characterized by the existence of strong bands at around 1170 and 690 cm
−1. Further weaker bands can be distinguished around 1270, 1100, 760, and 290–390 cm
−1. The strong and broad band at 1170 cm
−1 is assigned to the symmetric stretching mode of the PO
2− non-bridging bond in Q
2 groups. The feature at 1270 cm
−1 is related to the asymmetric stretch mode of PO
2−, V
as(PO
2−) in Q
2 groups. Q
1 units appeared through two weak shoulders at 1100 cm
−1 and 760 cm
−1, which are attributed to the symmetric stretching vibration of terminal PO
32− units, and to the symmetric stretching vibration of P–O–P, respectively. The band at 690 cm
−1 is attributed to the symmetric stretching mode of the P–O–P in Q
2 groups. Bands between 290 and 390 cm
−1 could be related, respectively, to bending vibrations of PO
2− and PO
32− [
38,
39,
41,
42,
43].
Figure 6 represents the FTIR spectra for the studied glasses in the range between 400 and 1400 cm
−1, which shows no significant difference between the four formulas; this indicated that the prepared glasses have similar chemical functional groups and similar chemical bonding. The feature at around 1290 cm
−1 is assigned to the asymmetric stretching of (PO
2−) in the phosphate tetrahedron Q
2, υ
as (PO
2−). The FTIR bands observed at 1155–1160 cm
−1 are characteristic of the symmetric stretching of (PO
2−) in Q
2 groups. The vibration of the band about 1100 cm
−1 is attributed to the υ
s PO
32− stretching vibrations, while the feature at 955–1080 cm
−1 is attributed to the stretching vibration υ
as O–P–O band in the phosphate tetrahedron Q
1. The two absorption peaks at 880 and 715 cm
−1 are attributed to asymmetric and symmetric stretching of the P–O–P in Q
2 groups, respectively. While the band at around 765 cm
−1 is assigned to the P–O–P stretching vibrations Q
1 species, bands between 550 and 480 cm
−1 are assigned to bending vibration of O–P–O and PO
32− bonds, respectively [
26,
38,
44].
Raman and FTIR spectra suggest that the structure of these vitreous fertilizers resembles metaphosphates, and the network is composed essentially of Q
2 units. However, the spectra also show the existence of Q
1 units, generally result in the presence of shorter phosphate chains, which can explain the appearance of several T
c and T
f during thermal analyzes.
Table 4 summarizes frequency ranges and assignments of the Raman and FTIR bands of the four glasses.
3.5. Dissolution Behavior
With increasing dissolution time in distilled water, the vitreous fertilizers exhibit an increased D
R, as revealed in
Figure 7. Chemical bonds between glass modifiers and glass formers are created due to the vitrification process. Consequently, if the glass stays undissolved, those modifiers cannot be liberated.
The dissolution of phosphate glass is the result of a set of complex mechanisms that depends not only on its physicochemical properties but also on the leaching conditions [
45]. When glass particles are in contact with water, processes of inter-diffusion, ion-exchange, reaction–diffusion, and hydrolysis take place. These processes involve three dissolution rate regimes: (i) Initial diffusion, which reflects the exchange between protons in leachate solution and glass network-modifier cations. At the beginning of dissolution, water particles permeate into the glass, mobile alkali modifier ions undergo diffusional ion exchange with protons in the solution; (ii) Hydrolysis process which involves the hydrolysis of P-O-M bonds (with M = P, Mg, Ca, Zn, Fe, etc.), constituting the network structure of a glass [
46]. Hydrolysis changes the phosphate network by attacking bridging bonds in the interphase formed by mobile elements’ release; and (iii) Rate drop, which is a transition between the initial rate and residual dissolution rate, as a result of the gradual saturation of the solution. This saturation induces a gradual rate decrease until a residual dissolution rate where the glass dissolution rate attains a relatively constant value, and thermodynamic equilibrium is approached—i.e., the chemical affinity for dissolution decreases [
45,
46].
The initial dissolution rates V
0 (V
0 =
of the linear part of the dissolution curves) are given in
Table 5. The chemical resistance of the glass is mainly dependent on its chemical composition. Formula F
0 showed the highest dissolution rate, while F
3 showed the lowest dissolution rate, followed by F
2 and F
1. The initial diffusion and hydrolysis process for F
0 lasted only two days, with an initial dissolution rate V
0 = 0.69 g/day. Almost the entirety was dissolved in water within less than four days. The degradation rate was found to decrease for F
1 and F
2 by incorporating iron and manganese into the glass matrix. The initial dissolution rates for these glasses were 0.14 and 0.17 g/day, respectively. The initial diffusion and hydrolysis process lasted between four and six days.
Hasan et al. [
47] have studied the chemical durability of P
2O
5-Fe
2O
3-Na
2O-CaO-MgO glasses and reported that Fe
2O
3 addition leads to the creation of more hydration resistant Fe-O-P bonds instead of P-O-P bonds, which increased cross-linking between the phosphate chains and improved the chemical durability of the glass.
Ahmina et al. [
48] suggested that by adding MnO to phosphate glasses, the chemical resistance was enhanced due to the increase in the cross-link between the phosphate chains by the formation of P–O–Mn bonds. These changes can be explained by the effect of cation substitution on the glass network structure. The addition of MnO causes the phosphate network to shrink and produce more entangled and networked metaphosphate chains.
In all the investigations above, MnO and Fe2O3 can both improve the durability of phosphate glasses; however, this study showed that Fe2O3 was much more effective in decreasing the initial degradation rate, while MnO had a greater effect on decreasing the residual rate. The admixture of Fe and Mn, in addition to other elements such as Zn, B, Cu, and Mo, in a phosphate glass network (F3) induces a rapid improvement in the chemical durability, which may be related to the strengthening of the bonds between non-bonding oxygen atoms and cations, leading to an overall network reticulation effect. The hydration process based on ion exchange between the cations in phosphate chains and water becomes thermodynamically less favorable with the increase of the cross-linking between the chains. Glass F3 has a V0 = 0.03 g/day; after 34 days, it had not yet reached the saturation stage, with a weight loss of only 71%.
Amounts of released elements from vitreous fertilizers to the leachate solution were determined using the ICP-OES, in the form of oxides normalized to the initial glass weight, and the pH measurements are presented in
Figure 8 and
Figure 9. The percentage of released ions increased over time. For F
0, amounts of P, K, Ca, and Mg in distilled water were significantly enhanced during the first two days of immersion. While for glasses F
1, F
2, and F
3, the effect of the addition of microelements, which resulted in a slower release of ions in water, has been noted. For the four glass formulations, the presence of entire elements in the analyzed solutions, with a percentage comparable to the glass composition, suggests that the glasses dissolved congruently, and no selective leaching occurred [
49]. The pH of the leachate solutions changed after immersion of glasses in distilled water. pH diminished linearly with dissolution time from 6.5 to attain the acidic range for all the studied fertilizers, then remained almost unchanged during periods of immersion. Previous studies showed the leachate solution’s pH varied with phosphate content of the immersed glass, with higher phosphorus contents in the solution resulting in lower pH values [
50]. However, even though formula F
0 releases more phosphorus, formula F
1 achieves a lower pH value. This can be explained by the fact that with the addition of iron, the metaphosphate chains are broken into smaller groups of short-chain phosphates such as P
4O
136−, P
3O
105− and P
2O
74−, which are linked to iron through P–O–Fe bonds [
51]. This phenomenon was not noted during the structural characterization by FTIR and Raman, which means that these short chains are in small quantities but have a remarkable effect on the pH.
3.6. Growth Parameters
The application of F
1 treatments mainly improved plant height, fresh and dry shoot weight, fresh ear weight, and the number of grains per plant, and the F
2 treatments mainly improved leaf area, fresh and dry root weight, and 1000 grain weight compared to the control and NPK treatments (
Table 6). On the other hand, the F
0 and F
3 treatments increased the root length and dry ear weight
, respectively, compared to the control and NPK treatments. Ouis et al. [
52] reported an improvement of ears, straw, grains, and maize yield under field conditions after applying vitreous fertilizers (SiO
2, P
2O
5, K
2O, Fe
2O
3, CuO). In addition, Abou-Baker et al. [
53] reported the same results using vitreous fertilizers containing the same elements in addition to ZnO and CuO.
Considering the maximum values of improvement, fresh and dry shoot weight, fresh ear weight, and the number of grains per plant showed a maximum improvement with the application of F
1 (F
1 R1 (30% to 58%) and F
1 R2 (18% to 61%)) (
Table 6). On the other hand, plant height and root length, fresh root weight, and weight of 1000 gain showed a maximum increase after the application of F
2 (F
2 R1 (23% to 64%) and F
2 R2 (23% to 159%)). In addition, root and ear dry weights and grain weight per plant showed a maximum improvement after the application of F
3 (F
3 R1 + N (63 to 188%) and F
3 R2 (85 to 140%)). The leaf area exhibited a maximum improvement after the application of F
0 R2 (28%). The positive effect of the vitreous fertilizers on growth traits (especially F
1 and F
2) could be explained by the high rates of release of different mineral elements contained in the vitreous fertilizers [
54].
3.7. Photosynthetic Parameters
The stomatal conductance (gs) and photosystem II efficiency (F
v/F
m) were increased by 32% and 13%, respectively, with the application of NPK fertilizer compared to the control. The gs was increased by 70% in plants treated with vitreous fertilizers (34% for F
0, 45% for F
1, 47% for F
2, and 107% for F
3) (
Table 6), while F
v/F
m was increased by 14% with the application of these fertilizers (11% for F
0, 13% for F
1, 16% for F
2, and 18% for F
3). The F
2 provided the highest percentages of improvement of these two parameters (151% (F
2 R1) and 116% (F
2 R2 + N) for gs and 24% (F
2 R2) for F
v/F
m). The improvements in these photosynthetic attributes by the application of vitreous fertilizers could be explained by the key role of these amendments in providing essential elements such as potassium, magnesium, copper, iron, and manganese, which are involved in many photosynthetic related processes and biomolecules, including stomata movements and photosynthetic pigments and enzymes. Ion et al. [
55] demonstrate that the application of vitreous fertilizers improved grapevine nutrition, in particular K and Mg uptake, which can stimulate many metabolism pathways, such as the regulation of stomatal exchanges as well as the balance of hormones such as ABA and thereby the photosynthesis functioning [
56]. The absorption of the essential nutrients included in the vitreous fertilizers boosts wheat growth and yield performances.
Based on the number of the improved parameters and the maximum values of this improvement, F1, F2, and F3 were distinguished in comparison to the control, NPK and F0 treatments especially with R2 application (1 g/plant). It seems that these three effective formulations could be suitable for a large-scale application in the open field to further investigate the performance of the applied vitreous fertilizers.